Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/11692
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dc.date.accessioned2018-04-11T07:13:29Zen
dc.date.available2018-04-11T07:13:29Zen
dc.date.issued2015en
dc.identifier.urihttp://hdl.handle.net/2122/11692en
dc.description.abstractThe presence of a seamount-like structure, located a few nautical miles offshore the Capo Vaticano Promontory (western Calabria, S Italy), was revealed by combined geophysical and geochemical investigation. The edifice covers ~55 km2, with a top located at a depth of about 70 m below sea level, and consists mainly of a NW-trending structure orthogonally interrupted by minor ridges, the largest of which is affected by extensional faults. The top of the edifice hosts active vents, injected fluids that have been investigated for dissolved volatiles. Gas analyses revealed high CO2 and CH4 contents, several orders of magnitude above the atmospheric-type values expected for shallow, coastal marine waters, and a noteworthy enrichment in mantle-derived 3He, which is an unambiguous indicator of the mantle origin of the fluids. Our results, combined with available data from the literature, suggest that the edifice is a tectonically controlled volcanic system, which presence near the Calabria region changes the role played by faults in the frame of the subduction process.en
dc.language.isoEnglishen
dc.relation.ispartofTerra Novaen
dc.relation.ispartofseries/27 (2015)en
dc.subjectSubmarine degassingen
dc.subjectdissolved gas geochemistryen
dc.subjectmantle degassingen
dc.subjectvolcanic structureen
dc.titleMantle degassing on a near shore volcano, SE Tyrrhenian Seaen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber195 – 205en
dc.subject.INGVMantle degassing on a near shore submarine volcano, SE Tyrrhenian Seaen
dc.identifier.doi10.1111/ter.12148en
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dc.description.obiettivoSpecifico5V. Dinamica dei processi eruttivi e post-eruttivien
dc.description.journalTypeJCR Journalen
dc.contributor.authorLoreto, Maria F.en
dc.contributor.authorItaliano, Francescoen
dc.contributor.authorDeponte, Davideen
dc.contributor.authorFacchin, Lorenzoen
dc.contributor.authorZgur, Fabrizioen
dc.contributor.departmentIstituto di Scienze Marine – Consiglio Nazionale delle Ricerche, Bologna, Italyen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Palermo, Palermo, Italiaen
dc.contributor.departmentIstituto Nazionale di Oceanografia e di Geofisica Sperimentale, Sgonico (TS), Italyen
dc.contributor.departmentIstituto Nazionale di Oceanografia e di Geofisica Sperimentale, Sgonico (TS), Italyen
dc.contributor.departmentIstituto Nazionale di Oceanografia e di Geofisica Sperimentale, Sgonico (TS), Italyen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptIstituto di Scienze Marine – Consiglio Nazionale delle Ricerche, Bologna, Italy-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Palermo, Palermo, Italia-
crisitem.author.deptIstituto Nazionale di Oceanografia e di Geofisica Sperimentale, Sgonico (TS), Italy-
crisitem.author.deptIstituto Nazionale di Oceanografia e di Geofisica Sperimentale, Sgonico (TS), Italy-
crisitem.author.deptIstituto Nazionale di Oceanografia e Geofisica Sperimentale, Sgonico (Trieste)-
crisitem.author.orcid0000-0003-1960-8684-
crisitem.author.orcid0000-0002-9465-6398-
crisitem.author.orcid0000-0001-8098-094X-
crisitem.author.orcid0000-0001-8141-9919-
crisitem.author.orcid0000-0002-7761-4110-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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